Changes between Version 6 and Version 7 of u/zchen/isothermalwind


Ignore:
Timestamp:
02/18/14 17:31:41 (11 years ago)
Author:
Zhuo Chen
Comment:

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  • u/zchen/isothermalwind

    v6 v7  
    99Substitute (3) and (2) into (1) and assume the wind is in steady state, we can get:
    1010
    11 $\frac{1}{u}\frac{du}{dt}=(\frac{2a^2}{r}-\frac{GM}{r^2})/(u^2-a^2)$  (4)
     11$\frac{1}{u}\frac{du}{dr}=(\frac{2a^2}{r}-\frac{GM}{r^2})/(u^2-a^2)$  (4)
    1212
    1313$u=a$ is a singular point and $\frac{2a^2}{r}-\frac{GM}{r^2}=0$ is critical point. If the wind is to experience constant acceleration, u will exceed a at some radius such that the equation become singular. Therefore the reasonable picture for the constant accelerating wind is that numerator goes to 0 as the denominator goes to 0.